阿尔及利亚霍达纳盆地中部地下水水质的水化学分析:一个案例研究

IF 0.9 Q4 ENVIRONMENTAL SCIENCES
Ahmed Ferhati, Ratiba Mitiche Kettab, Nour El Houda Belazreg, Hakim Djafer Khodja, Salim Djerbouai, Mahmoud Hasbaia
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引用次数: 2

摘要

本文的目的是确定矿化起源和区分不同类别的地下水质量在阿尔及利亚中部的半干旱盆地的几个地区。许多多元统计技术应用于由64个地理参考个体组成的数据集,其中包含19个化学变量。主成分分析结果表明,前5个因子解释了78%以上的地下水水质变异。其他方法,如CA聚类分析、CAH分层聚类分析和使用Piper图的地球化学分析,更适合考虑结核相发育和区分聚类。研究盆地的内源性特征决定了该盆地中心(Chott El Hodna)是一个盐度源。盐分从北到南逐渐升高,从无咸水到靠近乔特河的高咸水。结果表明,该地区的地下水是被描绘出来的,相确定评价表明,氯化钙、硫酸镁相占84%,其次是硫酸钠相,占14%,其余为碳酸氢盐相(2%)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrochemical analysis of groundwater quality in central Hodna Basin, Algeria: a case study
This paper aims to identify the mineralisation origin and distinguish between the different classes of groundwater quality in several regions of the semiarid basin of Hodna in central Algeria. Many multivariate statistical techniques are applied to a dataset composed of 64 georeferenced individuals with 19 chemical variables. The obtained results from this principal component analysis show that the first five factors explain more than 78% of the groundwater quality variance. Other methods such as CA cluster analysis, CAH hierarchical cluster analysis and geochemical analysis using the Piper diagram are more appropriate to contemplate nodule-facies development and to distinguish clusters. The endorheic characteristic of the study basin consequents the basin centre named Chott El Hodna to be a salinity source. Bit by bit, salinity raises from North to South, from unsalted water to strongly salted water close to the Chott. The outcomes demonstrate that this groundwater is portrayed, the facies definite assessment outlines that the chloride, calcium and magnesium sulphate facies indicate 84% of cases, trailed by sodium sulphate facies with 14% and the rest (2%) is identified by the bicarbonate facies.
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来源期刊
International Journal of Hydrology Science and Technology
International Journal of Hydrology Science and Technology Environmental Science-Environmental Engineering
CiteScore
2.50
自引率
5.60%
发文量
67
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